Effective seed dispersal is critical for enabling rapid state shift from a bare tidal flat to a vegetated marsh. While tidal currents are the main dispersal vector in coastal environments, biological characteristics that keep seeds afloat have been shown to influence primary seed dispersal, i.e., seed departure from the parent plant. In contrast, secondary seed dispersal processes that move (germinated) seeds trapped within microsites have been largely neglected. Here, we explore the extent to which the coupling between biotic traits and abiotic factors affects secondary seed dispersal, and whether secondary seed dispersal may explain sudden saltmarsh establishment (i.e., rapid colonization of bare tidal flat by large numbers of seedlings in spring). We used two widely spread pioneer species: Scripus mariqueter and Spartina alterniflora. Combined flume and field results demonstrated that: (1) germination stage, current velocity, and sedimentary regime have a marked effect on the probability of secondary seed dispersal by influencing the threshold lift-off velocity of (germinated) seeds within microsites; (2) density and bud length are critical biotic traits that best predict the potential of secondarydispersal onset after seed germination; (3) S. alterniflora possess a stronger secondary dispersal ability compared to S. mariqueter; and (4) secondary dispersal of germinated seeds in spring may explain observed sudden marsh establishment on bare tidal flats. Our findings provide novel insight relevant to understanding the drivers of seed dispersal and thereby sudden saltmarsh establishment events, with important implications for understanding the effects of climate change on critical state transitions and enabling human-aided restoration.Saltmarshes occur in near-shore coastal environments around the world (Barbier et al. 2011;Mcowen et al. 2017), and provide a multitude of valuable ecosystem services, such as habitat provisioning to unique species (Barbier et al. 2011), wave attenuation (Shepard et al. 2011Möller et al. 2014), and shoreline stabilization (Temmerman et al. 2013;Bouma et al. 2014). State shifts in this valuable ecosystem between low-lying bare mudflats and high-elevation vegetated marshes follow alternative stable state dynamics (Van Wesenbeeck et al. 2008;Marani et al. 2013;Wang and Temmerman 2013). Large-scale marsh collapse (i.e., the transition from vegetated marshes to mudflats) caused by ongoing anthropogenic and climatological disturbance has garnered widespread attention (Couvillion and Beck 2013;Kirwan et al. 2016;Hinshaw et al. 2017). In contrast, our understanding of the processes involving the transition from mudflats to vegetated marshes remains limited, despite its importance for the effective management and restoration of saltmarshes (Bouma et al. 2016;Cao et al. 2018Cao et al. , 2020.Saltmarsh plants can colonize large bare areas slowly by clonal expansion or quickly by establishing seedling cohorts (Zhu et al. 2020a). While clonal expansion is considered to be the main mechanism of...